Balogh Zoltán (szerk.): Neograd 2018 - A Dornyay Béla Múzeum Évkönyve 41. (Salgótarján, 2018)
Boglár-Marton Ágnes: Gravitációs tömegmozgások a csővári triász képződményekben (rövid összefoglaló)
RODRÍGUEZ-LÓPEZ, J. R, et al. 2007 „Lateral variability of ancient seismites related to differences in sedimentary facies (the synrift Escucha Formation, mid-Cretaceous, eastern Spain).” Sedimentary Geology 201(3-4): 461-484. SPALLUTO, L., et al. 2007 „Seismically-induced slumps in Lower-Maastrichtian peritidal carbonates of the Apulian Platform (southern Italy).” Sedimentary Geology 196(1-4): 81-98. SYVITSKI, J. P. M., et al. 2003 „Predicting the terrestrial flux of sediment to the global ocean: a planetary perspective.” Sedimentary Geology 162(1-2): 5-24. TRIPS AN AS, E. K„ et al. 2008 „Submarine mass-transport facies: new perspectives on flow processes from cores on the eastern North American margin.” Sedimentology 55(0): 97-136. ÁGNES BOGLÁR-MARTON GRAVITY FLOWS IN THE TRIASSIC FORMATIONS OF CSŐVÁR The aim of this study was to observe and describe the different gravity flows in sediment. This area (Csővár, Pokol-valley) is well known in Geology but scientists never examined it from this perspective. My study has several phases. First I observe the outcrop, then I describe the phenomenon of gravity flows, the succesion. Than I prepare thin sections in the laboratory for microscope analysis. During this analysis fossils were observed too. I was intrested whether the gravity flow had a preference which sediment affect or not. In my study I listed the gravity flow types, their characteristics and their presence in the outcrop. From the study occured, that in this area more different type of gravity flows are present (slump, turbidity current). From the measured layer dip data I could estimate which direction the transport happened into. 330